897 resultados para Randalls Island (N.Y.)--Maps, Topographic.
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Svalbard is a heavily glacier-covered archipelago in the Arctic. Dickson Land (DL), in the central part of the largest island, Spitsbergen, is relatively arid, and as a result, glaciers there are relatively small and restricted mostly to valleys and cirques. This study presents a comprehensive analysis of glacier changes in DL based on inventories compiled from topographic maps and digital elevation models for the Little Ice Age maximum (LIA), the 1960s, 1990 and 2009/11. Total glacier area decreased by ~38 % since the LIA maximum, and front retreat has increased over the study period. Recently, most of the local glaciers have been consistently thinning in all elevation bands, in contrast to larger Svalbard ice masses which remain closer to balance. The mean 1990–2009/11 geodetic mass balance of glaciers in DL is among the most negative from the Svalbard regional means known from the literature.
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In text: In 1986 the Statue will be 100 years old.
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Dissertação de Mestrado, Ciências Biomédicas, 28 de Junho de 2016, Universidade dos Açores.
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Cadastral survey map showing lot lines, lot nos., dimensions, acreages, and proposed streets.
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A commented and updated checklist of the hoverflies from the Mascarene island of Réunion, France, is presented. A total of 22 species are listed. New data on eight species are provided, two of them new to Réunion: Syritta austeni Bezzi, 1915 and Eristalinus madagascariensis (Hervé-Bazin, 1914). Réunion has 14 species shared with Madagascar and 10 with Mauritius. The present study contributes to better understand the biodiversity of this part of the world.
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This paper presents the determination of a mean solar radiation year and of a typical meteorological year for the region of Funchal in the Madeira Island, Portugal. The data set includes hourly mean and extreme values for air temperature, relative humidity and wind speed and hourly mean values for solar global and diffuse radiation for the period 2004-2014, with maximum data coverage of 99.7%. The determination of the mean solar radiation year consisted, in a first step, in the average of all values for each pair hour/day and, in a second step, in the application of a five days centred moving average of hourly values. The determination of the typical meteorological year was based on Finkelstein-Schafer statistics, which allows to obtain a complete year of real measurements through the selection and combination of typical months, preserving the long term averages while still allowing the analysis of short term events. The typical meteorological year validation was carried out through the comparison of the monthly averages for the typical year with the long term monthly averages. The values obtained were very close, so that the typical meteorological year can accurately represent the long term data series. The typical meteorological year can be used in the simulation of renewable energy systems, namely solar energy systems, and for predicting the energy performance of buildings.
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The research described in this thesis was motivated by the need of a robust model capable of representing 3D data obtained with 3D sensors, which are inherently noisy. In addition, time constraints have to be considered as these sensors are capable of providing a 3D data stream in real time. This thesis proposed the use of Self-Organizing Maps (SOMs) as a 3D representation model. In particular, we proposed the use of the Growing Neural Gas (GNG) network, which has been successfully used for clustering, pattern recognition and topology representation of multi-dimensional data. Until now, Self-Organizing Maps have been primarily computed offline and their application in 3D data has mainly focused on free noise models, without considering time constraints. It is proposed a hardware implementation leveraging the computing power of modern GPUs, which takes advantage of a new paradigm coined as General-Purpose Computing on Graphics Processing Units (GPGPU). The proposed methods were applied to different problem and applications in the area of computer vision such as the recognition and localization of objects, visual surveillance or 3D reconstruction.
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Let S(M) be the ring of (continuous) semialgebraic functions on a semialgebraic set M and S*(M) its subring of bounded semialgebraic functions. In this work we compute the size of the fibers of the spectral maps Spec(j)1:Spec(S(N))→Spec(S(M)) and Spec(j)2:Spec(S*(N))→Spec(S*(M)) induced by the inclusion j:N M of a semialgebraic subset N of M. The ring S(M) can be understood as the localization of S*(M) at the multiplicative subset WM of those bounded semialgebraic functions on M with empty zero set. This provides a natural inclusion iM:Spec(S(M)) Spec(S*(M)) that reduces both problems above to an analysis of the fibers of the spectral map Spec(j)2:Spec(S*(N))→Spec(S*(M)). If we denote Z:=ClSpec(S*(M))(M N), it holds that the restriction map Spec(j)2|:Spec(S*(N)) Spec(j)2-1(Z)→Spec(S*(M)) Z is a homeomorphism. Our problem concentrates on the computation of the size of the fibers of Spec(j)2 at the points of Z. The size of the fibers of prime ideals "close" to the complement Y:=M N provides valuable information concerning how N is immersed inside M. If N is dense in M, the map Spec(j)2 is surjective and the generic fiber of a prime ideal p∈Z contains infinitely many elements. However, finite fibers may also appear and we provide a criterium to decide when the fiber Spec(j)2-1(p) is a finite set for p∈Z. If such is the case, our procedure allows us to compute the size s of Spec(j)2-1(p). If in addition N is locally compact and M is pure dimensional, s coincides with the number of minimal prime ideals contained in p. © 2016 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim.
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Determination of Rare Earth Elements (REEs) in the waters and sediments of El Hito Lake and its drainage basin was carried out. Distribution maps for REEs concentrations show increasing values in the lake sediments from the center to the eastern edge reaching 166.5 mg/kg. In the drainage basin, higher values were observed with a maximum of 350.9 mg/kg in the southern part. Concentrations in the water were considerably lower with a maximum value of 1.3 µg/L. Ce, La and Nd were the most abundant elements. When normalized REE concentrations against NASC (North American Shale Composite), a positive anomaly of Eu in the water and of Nd in the sediments (lake and basin) was observed. The (La/Gd)NASC and (La/Yb)NASC ratios determined the predominance of light REE (LREE) over medium (MREE) and heavy REE (HREE). Key-words: Rare Earth Elements, lacustrine sediments and water, Eu anomaly, sulfates RESUMEN: Se llevó a cabo el estudio de Tierras Raras (REEs) del agua y los sedimentos de la Laguna de El Hito así como de su cuenca de recepción. Los mapas de distribución de las concentraciones de REE en los sedimentos de la laguna mostraron valores crecientes desde el centro hacia el margen este alcanzando 166.5 mg/kg. En la cuenca se midieron valores más elevados llegando hasta 350.9 mg/kg en la mitad sur. Los valores en el agua fueron notablemente inferiores, con un máximo de 1.3 µg/L. El elemento más abundante fue el Ce seguido del Nd. Se normalizaron las concentraciones de REEs frente a las del NASC (North American Shale Composite), observándose una anomalía positiva de Eu en el agua, así como de Nd en los sedimentos (laguna y cuenca). Mediante los índices (La/Gd)NASC y (La/Yb)NASC se determinó el predominio de las REEs ligeras (LREEs) frente a las medias (MREE) y pesadas (HREE).
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The purpose of the thesis for obtaining this PhD diploma is a comparative research between the origin of the Catalonian national movement and the Sardinian national one through the analysis of the 19th century periodicals as well as through a bibliography obtained by extracting them from consulted newspapers and magazines. Not only are both realities compared because of the Aragonese-Catalan influence over the Sardinian culture during its conquer but also because both movements had their origin during the 1840s and developed concurrently along that century presenting some differences, though. The political and cultural scene in Sardinia in those years was characterized by the spread of a discomfort feeling among the population after the acceptance of the “ Fusione perfetta” in 1848 and the following rollout of the “Statuto Albertino” in the island, representing this last regulation an attempt to unify the different Italian provinces in an administrative and legislative way, together with the previous “Feliciano” code from 1827. Therefore, this is how it began to be defined the set of political, economic, and cultural theme that forms the central point of the “questione sarda” (this term and its whole connotation were used for the first time in 1867 in an article published in the Cagliaritano weekly-publication La Cronaca). The singularity of this Sardinian nationalistic movement is related to the origin of the first regional demands expressed during those same years in some European regions and, more specifically, in Catalonia. Actually in this region, in those same years, we find the origin of a cultural movement called RenaixenÇa whose initial claim was the linguistic and cultural Catalonian renaissance and which adopted a more political meaning along the 19th century...
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The state of North Carolina is home to some of the most spectacular barrier islands in the world. These features are constantly shifting, impacted by waves, tides, and wind. Studies of the Outer Banks, North Carolina have resulted in varied results, but a detailed analysis of the barrier system as a whole is lacking. Using historic topographic surveys (T-sheets) from the 19th, the positions of various barrier segments were analyzed in relation to modern imagery. Changes in area, width, and center line locations were evaluated over the past 150 years. In total, 74 percent of modern transects have decreased in area. Total reductions in size were 130 km2 for the study period. Mean centerlines as a function of migration showed that 53 percent of segments were demonstrating directional movement away from the ocean. The average movement towards the bay between modern and historic centerlines was 8 meters. Thusly, barrier islands in North Carolina are demonstrating both decreases in total area and directional movement inland in response to sea level rise.
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Se efectuó la evaluación de bancos naturales de concha de abanico y pulpo del 7 al 16 de noviembre del 2009. La concha de abanico se distribuyó entre 06°21’07,8’’ y 06°26’04,4’’S al noreste de Cabo Cruz y sur de Peña Negra, con densidades absolutas de 1 a 178 ejem.m-2, en profundidades de 12 a 27 m; las tallas variaron entre 2 y 100 mm de altura valvar, media 41 mm, presentando moda principal en 37 mm y dos modas secundarias en 4 y 79 mm; predominaron ejemplares desovantes (37%) y madurantes (29%), se detectó el 26% de inmaduros. La biomasa de concha de abanico fue estimada en 8.877 t y la población en 865 millones de individuos. El stock de juveniles (<25 mm) fue 96 millones de ejemplares (11% de la población) y 36 t, el stock explotable (≥65 mm) fue 83 millones de individuos y 4.376 t. El pulpo se encontró pobremente distribuido en los alrededores de la isla; la talla varió entre 85 y 150 mm de longitud del manto. El 100% de lo capturado tuvo peso inferior al mínimo legal de extracción (1 kg). Hembras y machos estuvieron en estadios en desarrollo y maduros (66,67%).
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El objetivo general del Proyecto fue analizar, describir y conceptuar el comportamiento nictimeral y/o distribución de las principales especies de la comunidad pelágica del ecosistema de la sub-área antártica CCAMLR 48.1 en relación con la producción primaria, presencia de depredadores y condiciones físicas y químicas en la columna de agua. Para este fin se ejecutó un Crucero multidisciplinario en el estrecho de Bransfield y alrededores de la isla Elefante, durante enero del 2006
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The South Carolina Department of Natural Resources provides area maps of regions of the state that identify agency-owned and managed Wildlife Management Areas. This is a map of the Bear Island WMA.